不同磷水平配施生物炭对土壤磷有效性

生物炭在提高土壤磷素有效性及促进作物生长方面具有显著作用,但其效果因土壤类型不同存在较大差异。试验以赤红壤(pH 4.91)和褐土(pH 7.24)为供试土壤,设置3种磷肥水平(0、30、90 kg P·hm^-2,分别以不施磷、低磷、高磷表示)配施稻秆生物炭(0、4%)的大豆盆栽试验,研究了不同磷水平下配施生物炭对土壤磷有效性、磷酸单酯酶活性和植株磷吸收的影响。结果表明: 不同磷水平配施生物炭显著提高了两种土壤的速效磷和全磷含量,且低磷水平添加生物炭处理速效磷增幅最大,在赤红壤和褐土的增幅分别为192.6%和237.1%。与低磷相比,赤红壤中低磷配施生物炭处理的碱性磷酸单酯酶活性显著增加78.9%,活性有机磷含量降低39.3%,同时显著促进了植株生长与磷吸收;生物炭添加显著降低了褐土活性有机磷含量,但不同处理对土壤磷酸单酯酶活性和植株生长无显著影响。土壤活性有机磷含量与速效磷含量均呈显著负相关。综上,生物炭对土壤磷有效性的作用因土壤类型和磷肥水平差异而不同,其在赤红壤上对植株生长和磷吸收的促进效应强于褐土,且在低磷条件下效果更佳。本研究为生物炭在减施磷肥和促进大豆磷吸收,特别是在赤红壤上的应用提供了科学依据。     

不同磷源对磷高效利用野生大麦根际土壤磷组分的影响

在土培盆栽条件下,以野生大麦磷高效利用基因型IS-22-30、IS-22-25和低效基因型IS-07-07为材料,研究不施磷(CK)、无机磷(KH₂PO₄,Pi)、有机磷(phytate,Po)及二者混合(KH₂PO₄+phytate,Pi+Po)的方式施磷30 mg·kg^-1时,磷高效基因型野生大麦对磷素吸收利用能力及土壤磷组分特征.结果表明： Pi处理野生大麦干物质量和磷素积累量最大,Pi+Po处理其次,Po处理最小,均显著高于CK处理,且磷高效基因型物质生产和磷素吸收能力显著高于磷低效基因型.土壤有效磷在不同磷源处理间差异显著,Pi处理时含量最高,Pi+Po处理次之,且磷高效基因型野生大麦根际有效磷含量显著高于磷低效基因型.磷高效基因型野生大麦根际有效磷呈现亏缺现象,在Pi和Pi+Po处理时亏缺程度较大.根际与非根际土壤无机磷组分含量为Ca₁₀-P>O-P>Fe-P>Al-P>Ca₂-P>Ca₈-P,且其含量随着Pi的增加而增加.各磷源处理下,磷高效基因型野生大麦根际土壤Ca₂-P、Ca₈-P出现亏缺;Pi处理磷高效基因型野生大麦根际土壤Al-P、Fe-P出现富集.土壤中有机磷各组分含量为中活性有机磷>中稳性有机磷、高稳性有机磷>活性有机磷.野生大麦根际土壤活性有机磷和中活性有机磷呈现富集,其富集量在Pi处理时最大;中稳性有机磷和高稳性有机磷呈现亏缺.各磷源处理下,磷高效基因型野生大麦根际土壤活性有机磷含量显著高于磷低效基因型,中稳性有机磷和高稳性有机磷在基因型间差异不显著.Pi缺乏时,磷高效基因型野生大麦活化吸收Ca₂-P、Ca₈-P、Al-P和活性有机磷的能力较强.     

磷肥输入对稻田土壤剖面胶体磷含量的影响

磷肥管理与土壤磷素赋存息息相关,选取杭嘉湖地区典型稻田定位实验,研究磷肥输入下稻田土壤剖面胶体磷含量的变化,分析不同施肥管理下胶体磷在土壤中的分布规律。结果表明,(1)胶体磷是磷素在土壤中赋存的重要形式,能够占到土壤胶体溶液(1μm)总磷的85%以上,土壤全磷的0.1%—2%;(2)磷肥施用增加了土壤胶体磷含量,特别是在有机肥处理下0—5 cm土壤胶体磷含量达到了8.0 mg/kg;(3)随着土壤深度的增加,胶体磷含量减少,有机肥输入下对深层土壤胶体磷含量的影响较无机肥明显;(4)水稻收割后表层土壤胶体磷含量与油菜收割后相比减少明显,0—5 cm土壤胶体磷含量减少了90%左右,但有机肥施用下胶体磷含量减少较小;(5)水稻收割后30—60 cm土壤胶体磷含量有所增加,可能与胶体磷发生的纵向迁移有关。了解磷肥输入对稻田土壤剖面胶体磷含量的影响,为研究土壤磷素赋存形态及迁移变化提供科学依据,对有效评估胶体磷的环境风险起到指导作用。     

Changes in soil phosphorus fractions following positive and negative phosphorus balances for long periods

The effect of phosphorus (P) balance (addition, in both fertilizers and farmyard manure (FYM), minus removal in crops) on eight soil P fractions determined by sequential extraction, was measured on archived soils from various long-term experiments run by Rothamsted Experimental Station in the United Kingdom. It has been established unequivocally that, for all the soils investigated, no one of the eight P fractions was increased or decreased during long periods of P addition or depletion, respectively. However, changes were mainly in the resin (24–30%) and the inorganic (P_i) component of the four fractions extracted sequentially by 0.5 M NaHCO₃, 0.1 M NaOH, 1.0 M NaOH, 0.5 M H₂SO₄ (41–60%). For the sandy loam there were also consistent changes in the organic (P_o) fraction (25%), especially that extracted by bicarbonate, presumably because the soil contained only a little clay and presumably had low sorption capacity. When the soils were cropped without P addition the largest proportional change was in the P extracted by resin, 0.5 M NaHCO₃ and 0.1 M NaOH, suggesting that the P in these fractions is readily available, or has the potential to become available, for crop growth. This was supported by changes in the overall P balance. On the heavier textured soils, 50–80% of the change in total soil P (P_T) was in these fractions; on the sandy soil this increased to more than 90%. The change in the sum of the first five fractions accounted, on average, for 90% of the P balance. However these changes in the P in the plough layer frequently left large amounts of P unaccounted for in some of the excessively P enriched soils. The amount of P_i extracted by resin and bicarbonate (P_i(r+b)) ranged between 14 and 50% of the sum of the P_i fractions. Soils with the lower percentages were those known to be most responsive to P fertilizers. P_i(r+b) accounted for an average of 70% of the P balance (negative) in P depleting soils where crop offtake was not offset or exceeded by annual P additions (positive balance). The ratio between P_i(r+b) and P_i(sum) could be a guide in defining soils deficient in P and those which are excessively enriched.     

不同施磷量对春油菜产量和土壤磷素平衡的影响

青海省东部春油菜主产区的土壤速效磷含量高、磷肥施用量大、磷肥利用率低。研究不同施磷量对春油菜的生长、磷素吸收和利用、土壤磷素平衡的影响,可为该地区春油菜田养分高效管理提供科学依据,对保障青藏高原农业可持续发展具有重要意义。本研究于2017和2018年在青海省互助县开展了田间试验,设置0、30、60、90、120 kg P₂O₅·hm^-2 5个磷肥施用量,测定了不同处理春油菜的产量、磷素吸收与利用、籽粒含油率等。结果表明: 2017年施磷量60 kg·hm^-2处理的油菜籽粒产量、成熟期地上部磷素累积量和产油量均显著高于不施磷处理,但施磷量超过60 kg·hm^-2后,籽粒产量和产油量不再增加;2018年施磷量对春油菜籽粒产量、成熟期地上部磷素累积量和产油量均无显著影响。两年度的磷肥表观利用率均很低,平均为6.7%。施用磷肥条件下土壤均有不同程度的磷素盈余,施磷量低于60 kg·hm^-2时盈余量较低。综合考虑春油菜产量、产油量、磷肥表观利用率和土壤磷素表观平衡,在青海省东部春油菜区,推荐施磷量为60 kg·hm^-2。     

施磷对川西北高寒草地土壤磷形态及有效性的影响

以川西北高寒草地为研究对象,采用随机区组设计,设置0、10、20、30、40、50、60 g/m²的过磷酸钙(P₂O₅,16%)施肥试验,分析土壤不同形态磷含量和有效磷(Olsen-P)含量变化特征,探究施磷对川西北高寒草地土壤磷形态及有效磷的影响。结果表明：(1)随施磷量增加,土壤总磷(TP)含量先增加后趋于平稳而Olsen-P含量减少。高水平(50、60 g/m²)施磷下氢氧化钠有机磷(NaOH-Po)及残留磷(Residual-P)是高寒草地主要的磷素累积形态,其含量显著高于不施磷处理;(2)树脂交换态磷(Resin-Pi)、碳酸氢钠无机磷(NaHCO₃-Pi)、碳酸氢钠有机磷(NaHCO₃-Po)和氢氧化钠无机磷(NaOH-Pi)含量随施磷量增加整体呈先增加后降低趋势,表层土壤30 g/m²磷肥用量下其值均为最高,分别为21.54、22.94、65.86、64.48 mg/kg。酸溶性无机磷(HCl-Pi)随施磷量增加整体呈下...     

Understanding plant responses to phosphorus starvation for improvement of plant tolerance to phosphorus deficiency by biotechnological approaches

Abstract

In both prokaryotes and eukaryotes, including plants, phosphorus (P) is an essential nutrient that is involved in various biochemical processes, such as lipid metabolism and the biosynthesis of nucleic acids and cell membranes. P also contributes to cellular signaling cascades by function as mediators of signal transduction and it also serves as a vital energy source for a wide range of biological functions. Due to its intensive use in agriculture, P resources have become limited. Therefore, it is critically important in the future to develop scientific strategies that aim to increase P use efficiency and P recycling. In addition, the biologically available soluble form of P for uptake (phosphate; Pi) is readily washed out of topsoil layers, resulting in serious environmental pollution. In addition to this environmental concern, the wash out of Pi from topsoil necessitates a continuous Pi supply to maintain adequate levels of fertilization, making the situation worse. As a coping mechanism to P stress, plants are known to undergo drastic cellular changes in metabolism, physiology, hormonal balance and gene expression. Understanding these molecular, physiological and biochemical responses developed by plants will play a vital role in improving agronomic practices, resource conservation and environmental protection as well as serving as a foundation for the development of biotechnological strategies, which aim to improve P use efficiency in crops. In this review, we will discuss a variety of plant responses to low P conditions and various molecular mechanisms that regulate these responses. In addition, we also discuss the implication of this knowledge for the development of plant biotechnological applications.     

长期施磷对玉米-小麦轮作系统作物产量和磷素吸收及土壤磷积累的影响

本研究利用位于河北省保定市的7年田间定位试验,探讨了4个磷水平(不施磷、70%优化施磷、优化施磷、130%优化施磷)对玉米-小麦轮作系统作物产量的影响,分析了作物磷素吸收和磷肥利用效率以及土壤磷盈亏的变化。结果表明: 长期(7年)施磷能够显著提高玉米和小麦产量及磷素吸收量,且玉米和小麦产量与磷素吸收量随着施磷量的增加均呈现先上升后下降的抛物线变化趋势。各施磷水平下玉米季磷肥利用率高于小麦季,小麦季磷肥累积利用率呈现下降趋势,下降速率表现为优化施磷>70%优化施磷>130%优化施磷;玉米季磷肥累积利用率均呈现上升趋势,上升速率表现为优化施磷>70%优化施磷>130%优化施磷。长期不施磷条件下土壤表观磷盈亏量和累积磷盈亏量都表现为亏缺状态,施磷条件下土壤磷表现为盈余,且施磷量越高,累积年限越长,土壤磷盈余量越高。河北潮土在秸秆还田条件下小麦施磷量在105～150 kg·hm^-2,玉米施磷量在63～90 kg·hm^-2时,既能保证作物高产,又能使磷肥利用率保持在较高水平,减少磷素在土壤中的累积,降低环境风险。     

Engineering microalgae for water phosphorus recovery to close the phosphorus cycle

As a finite and non-renewable resource, phosphorus (P) is essential to all life and crucial for crop growth and food production. The boosted agricultural use and associated loss of P to the aquatic environment are increasing environmental pollution, harming ecosystems, and threatening future global food security. Thus, recovering and reusing P from water bodies is urgently needed to close the P cycle. As a natural, eco-friendly, and sustainable reclamation strategy, microalgae-based biological P recovery is considered a promising solution. However, the low P-accumulation capacity and P-removal efficiency of algal bioreactors restrict its application. Herein, it is demonstrated that manipulating genes involved in cellular P accumulation and signalling could triple the Chlamydomonas P-storage capacity to ~7% of dry biomass, which is the highest P concentration in plants to date. Furthermore, the engineered algae could recover P from wastewater almost three times faster than the unengineered one, which could be directly used as a P fertilizer. Thus, engineering genes involved in cellular P accumulation and signalling in microalgae could be a promising strategy to enhance P uptake and accumulation, which have the potential to accelerate the application of algae for P recovery from the water body and closing the P cycle.     

低磷胁迫下磷高效基因型大麦的根系形态特征

在根袋土培盆栽条件下,以磷高效基因型DH110+、DH147和低效基因型DH49大麦为试验材料,利用根系分析系统分析不同施磷(P₂O₅)水平(极低磷25 mg·kg^-1、低磷50 mg·kg^-1和正常磷75 mg·kg^-1)下,磷高效基因型大麦的根系形态特征及其与植株磷素吸收的关系.结果表明： 低磷胁迫显著降低大麦生物量和磷吸收量,其中磷高效基因型的生物量和磷吸收量在各施磷水平下分别为低效基因型的1.24～1.70和1.18～1.83倍;大麦的总根长、总根表面积、平均根系直径、不定根长及其根表面积、侧根长及其根表面积均随施磷水平的降低而显著降低,其中磷高效基因型大麦在各施磷水平下的总根长、总根表面积、比根长、侧根长及根表面积分别为低效基因型的1.46～2.06、1.12～1.51、1.35～1.72、1.69～2.42和1.40～1.78倍,而平均根系直径为低效基因型的70.6%～90.2%;主成分分析表明,平均根系直径、比根表面积和比根长受基因型差异的影响较为明显,是区分两类磷效率基因型大麦根系形态差异的主要指标;偏最小二乘回归分析表明,各施磷水平下,总根长、总根表面积对大麦植株磷素吸收贡献均较大,随施磷水平降低,不定根长、不定根表面积对大麦植株磷素吸收的贡献明显降低,而平均根系直径、比根长、侧根长及其根表面积的贡献明显增加.磷高效基因型大麦可通过维持侧根的生长、根细度和比根长的增加来适应低磷胁迫.     

Reducing carbon: phosphorus ratio can enhance microbial phytin mineralization and lessen competition with maize for phosphorus

We tested the hypothesis that reducing the carbon (C):Phosphorus (P) ratio in rhizosphere soil would reduce bacterial competition with the plant for P from phytin, which would then increase phytin use efficiency for the plant. A three-factor pot experiment was carried out to study the effect of inoculation with a phytin-mineralizing bacterium, Pseudomonas alcaligenes (PA), on maize P uptake from phytin. Two levels of organic P, two levels of inorganic P, and three different PA inoculation treatments were used. When maize plants were grown in low available P soil with phytin, PA transformed soil P into microbial biomass P, which caused competition for available P with plant and inhibited plant uptake. When 5 mg P kg^?1 as KH₂PO₄ was added, inoculation with PA increased soil acid phosphatase activity which enhanced the mineralization rate of phytin. PA mobilized more P than it immobilized in microbial pool and enhanced plant P uptake. We conclude that the decreased C:P ratio by adding small amount of inorganic P in the rhizosphere could drive phytin mineralization by the bacteria and improve plant P nutrition.     

长期施肥对石灰性土壤磷素肥力的影响 Ⅰ.有机质、全磷和速效磷

在陕西关中黄土区连续23年进行了不同施肥、小麦玉米轮作定位试验,研究了0～100cm土层土壤有机质、全磷、速效磷含量变化.结果表明,长期单施化肥或有机肥与化肥且配施均可增加耕层(0～20cm)土壤有机质含量.长期施用厩肥并配施化肥处理对土壤总磷库及无机磷库、速效磷的贡献大于玉米秸秆处理.长期单施化肥可增加土壤全磷、无机磷和速效磷含量,增加幅度低于厩肥和休闲处理,与秸秆处理对全磷、速效磷含量的影响效应相近.23年的不同施肥处理,与无肥处理相比,其理土壤磷素增量在0～100cm土壤剖面中的分布特点是:全磷增量剖面分布可为3层———耕层(0～20cm)为显著累积层,20～60cm土层为微增-亏损层,60～100cm土层为轻度累积层.速效磷增量剖面分布趋势与全磷增量分布趋势基本相同,仅在60～100cm土层累积较弱.     

供磷水平及方式对杉木幼苗根系生长和磷利用效率的影响

为研究杉木幼苗根系生长、形态学指标及养分利用效率对土壤磷素异质分布的响应规律,选择杉木种子园单株采种培育的半同胞家系实生幼苗为研究对象,采用室内沙培控磷盆栽试验,设计低浓度供磷(8 mg/kg KH_2PO_4)、正常供磷(16 mg/kg KH_2PO_4)和高浓度供磷(32 mg/kg KH_2PO_4)3个供磷水平,每个供磷水平分别采用2种供磷方式(局部供磷和均匀供磷)进行根部施磷。结果表明:(1)从供磷水平来看,低浓度供磷下的杉木根长、根系生物量、根冠比、根系及全株的磷素利用效率均显著大于正常供磷和高浓度供磷,而根平均直径相反;随着供磷水平的提高,杉木苗高和地上部生物量无显著差异,而比根长表现出逐渐降低的趋势。(2)从供磷方式来看,局部供磷处理的杉木苗高、根长、根系表面积、比根长、地上部生物量、根系及全株的磷素利用效率均显著大于均匀供磷处理,而根平均直径和根冠比则相反。总体上,低浓度局部供磷处理下杉木可明显增强其根系的形态可塑性,从而优化根系在养分异质土壤里的空间分布,并通过提高根系磷素利用效率以维持地上部的正常生长。     

长期施肥对石灰性土壤磷素肥力的影响Ⅰ．有机质、全磷和速效磷

在陕西关中黄土区连续23年进行了不同施肥、小麦-玉米轮作定位试验。研究了0～100cm土层土壤有机质、全磷、速效磷含量变化．结果表明,长期单施化肥或有机肥与化肥且配施均可增加耕层(0～20cm)土壤有机质含量．长期施用厩肥并配施化肥处理对土壤总磷库及无机磷库、速效磷的贡献大于玉米秸秆处理．长期单施化肥可增加土壤全磷、无机磷和速效磷含量,增加幅度低于厩肥和休闲处理,与秸秆处理对全磷、速效磷含量的影响效应相近．23年的不同施肥处理,与无肥处理相比,其理土壤磷素增量在0～100cm土壤剖面中的分布特点是：全磷增量剖面分布可为3层——耕层(0～20cm)为显著累积层,20～60cm土层为微增一亏损层,60～100cm土层为轻度累积层．速效磷增量剖面分布趋势与全磷增量分布趋势基本相同,仅在60～100cm土层累积较弱．     

聚磷茵JPA1菌株的生长特性和聚磷条件的优化

以YG培养基为基础,考察不同条件对聚磷菌JPA1菌株生长及聚磷效率的影响。结果表明：JPA1菌株生长的对数期为3-9h,9h后进入稳定期,12h到达衰亡期。在单因素试验中,麦芽糖为JPA1菌株最适生长和聚磷的C源,最适生长温度为30-35℃,pH为8,Na＋、Ca2＋、Mg2＋、Mn2＋和K＋等离子有利于JPA1菌株的生长;最适聚磷温度为30-35℃,pH为7,Fe2＋、Na2＋、Mg2＋、Mn“和K＋等离子有利于JPA1菌株的聚磷。正交试验结果表明：JPA1菌株去磷培养基的最优组合为麦芽糖1．5g／L,温度37℃,pH6．5,装液量50mL（300mL摇瓶）;菌株最适扩增培养基为麦芽糖1．5g/L,温度37℃,pH6．5或7．5,装液量150mL（300mL摇瓶）。     

Distribution and release of sedimentary phosphorus in Lake Ladoga

Sedimentary phosphorus fractions and phosphorus release from the sediments were studied in Lake Ladoga at altogether 46 sampling sites, representing the full range of sediment types encountered in the lake. Determination of P fractions and physico-chemical analyses were made of surface sediment cores (10–20 cm long, each sampled at 3–4 levels) and in the overlying water. The range of total phosphorus per dry weight of sediment was 0.2–3.3 mg g^–1, and that of inorganic P 0.1–2.5 mg g^–1. The levels of interstitial soluble phosphorus, range 2–613 µg 1^–1 for total P and 1–315 µg 1^–1 for inorganic P, were higher than those of dissolved P concentrations in the overlying water. Diffusive fluxes of phosphate from sediment to the overlying water were estimated using three independent methods. The estimated range was 4–914 µg P m^–2 d^–1; the mean value for the whole bottom area, 0.1 mg P m^–2 d^–1, is lower than previously published estimates. The estimated annual contribution of sedimentary inorganic P flux to Lake Ladoga water is equal to 620 tons of P per year, which amounts to more than 10% of the estimated external P load into the lake. 68% of the total diffusive flux emanates from deep water sediments, which are not exposed to seasonal variation of conditions. In deep lakes, such as Lake Ladoga, phosphorus release from the sediments is controlled primarily by diffusive mechanisms. Wave action and currents as well as bioturbation are probably of importance mainly in shallow near-shore areas. Phosphorus release by gas ebullition and macrophytes is considered negligible.     

中亚热带森林更新方式对土壤磷素的影响

为了深入了解磷(P)在中亚热带森林生态系统内的有效性,在三明市梅列区陈大采育场黄坑工区,选择天然林采伐后采取不同更新方式的多种森林,以米槠天然林为对照,研究森林不同更新方式对中亚热带森林土壤全磷、有效磷及可溶性有机磷的影响。结果显示:在0—100 cm土层,(1)土壤全磷平均含量大小顺序依次为米槠天然林(NF)(0.49±0.09)g/kg,米槠轻度干扰人促更新林(LAR)(0.35±0.04)g/kg,米槠强度干扰人促更新林(HAR)(0.34±0.03)g/kg,马尾松人工林(PIM)(0.32±0.02)g/kg,杉木人工林(CUL)(0.3±0.03)g/kg,人促更新林比人工林高,NF显著高于其它的林分(P0.05);(2)土壤有效磷(Na HCO3提取)平均含量大小顺序依次为NF(0.41±0.39)mg/kg,LAR(0.26±0.2)mg/kg,HAR(0.23±0.16)mg/kg,PIM(0.17±0.05)mg/kg,CUL(0.13±0.06)mg/kg,NF显著高于其它林分,LAR显著比人工林高(P0.05)。(3)在0—10 cm土层,各林分可溶性有机磷含量在夏季最高,冬季最低,温度和降水量的季节变化是影响其重要因子之一;同一季节,人促更新林比人工林高,NF显著高于人工林(P0.05)。结果表明,全磷、有效磷和可溶性有机磷含量随人为干扰强度的增强呈降低趋势,其与年凋落物量和土壤有机碳储量呈显著正相关,与土壤容重呈显著负相关,全磷和有效磷在土壤剖面呈表聚性特征。相比于人工林经营,采取人促天然更新的方式,更有利于中亚热带森林养分的贮存和转化,有利于森林的长期经营和管理。     

Induction of maize acid phosphatase activities under phosphorus starvation

Large variation in phosphorus-(P) acquisition efficiency exists among maize inbred and hybrid genotypes. Acid phosphatases are a type of enzyme that affects P acquisition and P-use efficiency in plants. The objectives of this research were (1) to characterize acid phosphatase activity in maize grown hydroponically under P starvation, and (2) to determine if there is differential induction of acid phosphatases in two maize genotypes previously characterized as P efficient (Mo17) and P inefficient (B73). B73 and Mo17 seedlings were grown hydroponically and both intracellular and secreted acid phosphatase activities were characterized. Fresh seedling weight of both genotypes decreased under P starvation, but percent fresh weight allocated to roots increased 14 days after P starvation in B73. Soluble protein concentration in shoots and roots was affected little, but secreted protein decreased by 40 and 20% in B73 and Mo17 seedlings grown without P for 14 days. Intracellular and secreted acid phosphate activity increased substantially in leaves and roots in B73 and Mo17 in response to P starvation. Secreted APase activity per unit protein increased 310 and 300% in B73 and Mo17, respectively, 7 days after P withdrawal. One of the minor isozymes identified on non-denaturing PAGE, was increased specifically in response to P starvation in both maize genotypes. The patterns and levels of change in APase activities in B73 and Mo17 were not sufficiently different to account for the diverse growth response of these genotypes in low-P conditions. The results suggest that APases may not be a major mechanism for scavenging or acquiring P and changes in APases may reflect a state of P stress in both varieties. Other factors such as root architecture, secretion of low-molecular weight carboxylates and microbial interactions might explain the difference between these two genotypes.     

甘蔗幼苗对难溶性磷的吸收及其根系对低磷胁迫的响应

为明确甘蔗适应低磷胁迫的生理生化机制,挖掘甘蔗对磷素的利用潜力,揭示甘蔗对低磷胁迫适应的可能机制,该研究以ROC22和ROC10两个甘蔗品种为材料,采用水培和土培的方法研究了甘蔗幼苗对难溶性磷的吸收及其在低磷胁迫下根构型和根系的生理反应。结果表明:(1)培养在以难溶性磷(Ca-P和Al-P)为磷源的培养液中的甘蔗的叶片数、地上部干重、生物量较缺磷(-P)处理显著增加,与对照(+P)的相当,甘蔗总磷积累量也显著提高,达到对照(+P)处理磷积累量的30%～77%。(2)在低磷条件下,甘蔗幼苗的根系有向土壤深层分布的趋势,根的总体积增大、最长根长变长、浅根系分布增多。(3)甘蔗幼苗在低磷环境下,根际环境明显酸化,且根系分泌物能溶解难溶性的铝磷,植株体内酸性磷酸酶的活性也明显增强。以上表明甘蔗幼苗有较强的吸收利用难溶性磷的能力,而低磷条件下根系数量增加、主根的向地性、浅根系分布增多、根际酸化以及植株体内酸性磷酸酶活性的增强可能是甘蔗幼苗适应缺磷环境的重要机制。     

固磷基质(无定形铁)淋失特征及其与磷素淋失的关系

采用淋洗试验研究了水田土壤固磷基质（无定形铁）淋失特征及其与磷素淋失的关系。结果表明,添加柠檬酸和葡萄糖培养处理对无定形铁、络合态铁的淋失具有极显著效应,水分和温度等因素对无定形铁和络合态铁的淋失交互效应显著;相关分析表明,固磷基质（无定形铁）淋失与磷素淋失的相关关系显著,说明对磷素淋失有一定的影响。